Phaneritic Texture
igneous rock texture in which minerals are easily visible without magnification (indicates a long time to cool)
Aphanitic Texture
A texture of igneous rocks in which the crystals are too small for individual minerals to be distinguished without the aid of a microscope (indicates fast cool time)
Porphyritic Textrue
an igneous texture consisting of large crystals embedded in a matrix of much smaller crystals (typically this rock started cooling underground and was disturbed causing it to finish cooling quickly above ground)
Vesicular Texture
ingeous rock texture that has a lot of holes & bubbles (these rocks are often formed from ash)
Pyroclastic Texture
an igneous rock comprised of a bunch of ash & crystal grains
Glassy Texture
An igenous texture formed when a rock cools so fast it doesn't have time to crystallize, rather it forms a smooth glassy surface (typically found from surfaces of lava flows)
Adamantine Luster
exceptionally bright and reflective (diamond)
Vitreous Luster
shines like glass
Sub-Vitreous Luster
slightly less shiny than glass
Pearly Luster
looks like a pearl, a reserved sort of sheen
Silky Luster
shines like silk, the surface of the mineral is slightly textured
Greasy Luster
surface of the mineral looks covered in grease
Earthy Luster
mineral is naturally very dull, no shine
Amphibole (Hornblende)
a mineral with vitreous luster, is dark green/black in color (mafic), grey/white streak, hardness of 5/6
Biotite (Mica)
a mineral with viterous luster, is dark brown/black in color (mafic), greay streak, hardness of 2.2/3, and has cleavage in 1 perfect direction
Calcite
a mineral with vitreous luster, can be many colors, white streak, hardness of 3, and has 3 perfect planes of cleavage
Feldspar
a mineral with viterous luster, is pink/white/grey in color, white streak, hardness of 6/6.5
Fluorite
a mineral with vitreous luster, is green/blue/purple in color, white streak, hardness of 4, and fractures in uneven flat surfaces while having 4 planes of cleavage
Graphite
a mineral with sub-metalic luster, is grey in color, dark grey streak, hardness of 1.5/2, often used for pencils
Gypsum
a mineral is white or clear in color, white streak, hardness of 2
Halite (Salt)
a mineral with a greasy luster, is clear or white in color, white streak, hardness of 2.5, and has perfect cleavage in 3 directions
Hematite
a mineral with either a metalic or earthy luster, is grey/brown/red in color, maroon streak, hardness of 6.5, has weak magnetism
Magnatite
a mineral with a metalic luster, is grey/black in color, hardness of 5.5/6, cleavage in one direction, is strongly magnetic
Muscovite (Mica)
Vitreous luster, light brown/clear in color (felsic), white streak, hardness of 2.5/3, perfect cleavage in one direction
Olivine
vitreous luster, green color (mafic), white streak, hardness of 6
Pyrite
metalic luster, brass yellow color, green/gray/black streak, hardness of 6.5
Pyroxene
vitreous luster, mafic coloring, green streak, hardness of 5, 2 planes of perfect cleavage
Quartz
vitreous luster, any color, white streak, hardness of 7, conchoidial fracture
Talc
pearly/greasy luster, white color and streak, hardness of 1
Granite
igneous rock with phaneritic texture and felsic composition
Diorite
igneous rock with phaneritic texture and intermediate composition
Gabbro
igneous rock with phaneritic texture and mafic composition
Rhyolite
igneous rock with aphanitic texture and felsic composition
Andesite
igneous rock with aphanitic texture and intermediate composition
Basalt
igneous rock with aphanitic texture and mafic composition
Pumice
igneous rock with a vesicular texture and felsic composition
Scoria
igneous rock with a vesicular texture and mafic composition
Vesicular Basalt
igenous rock with a vesicular texture and mafic composition, however this rock is much heavier than its vesicular rock counterparts
Porphyritic Andesite
igneous rock with porphyritic texture and intermediate composition
Volcanic Tuff
igneous rock with pyroclastic texture & mafic to felsic composition
Obsidian
igneous rock with glassy texture and mafic composition
Clastic Sedimentary Rock
composed of other rock fragments cemented by silicate minerals, grain size dictates what the name of the rock is
Biochemical Sedimentary Rock
composed of organisms and material that dissolved in solution to form a rock, often are very reactive to acid
Organic Sedimentary Rock
composed of dead organisms
Breccia
clastic rock with large, angular, poorly sorted grains
Conglomerate
clastic rock with large, rounded, poorly sorted grains
Sandstone
clastic rock with course, rounded, well sorted sand grains
Shale
clastic rock with fine, rounded, well sorted mud & clay grains
Coquina
biochemical rock composed of shell fragments, reacts with acid
Fossiliferous Limestone
biochemical rock that is poorly sorted, contains fossils, acid reactive
Microcrystaline Limestone
biochemical rock that is well sorted, acid reactive
Chalk
biochemical rock composed of fine shell fragments, acid reactive
Coal
organic rock, there are different stages , the youngest being called peat
Rock Gypsum
very soft chemical rock, is an evaporite
Rock Salt
chemical rock made up of halite, is an evaporite
Chert
chemical rock that is composed of icrocrystaline quartz, is NOT acid reactive
Slate
low grade metamorphic rock, shale protolith
Phyllite
low grade metamorphic rock, satin luster, slate protolith
Schist
medium grade metamorphic rock, glittery shiny luster, phyllite protolith
Gneiss
high grade metamorphic rock, clear foliation and distinct banding of dark and light minerals, schist protolith
Migmatite
high grade metamorphic rock, experiences some partial melting, migmatite protolith
Quartzite
recrystalized quartz crystals, sandstone protolith
Marble
recyrstalized calcite, limestone protolith
Chemical Sedimentary Rock
forms when minerals become supersaturated in a solution and precipitate to form a rock